Cyclic characteristics of sediments in the Moon Island Beach Subgroup, Newcastle Coal Measures, New South Wales

1973 ◽  
Vol 5 (1) ◽  
pp. 91-110 ◽  
Author(s):  
K. R. Johnson ◽  
A. C. Cook
1918 ◽  
Vol 5 (7) ◽  
pp. 289-293
Author(s):  
R. Etheridge ◽  
A.C. Seward

In 1849 Professor J. D. Dana described certain leaves from the Illawarra District and Newcastle, New South Wales, occurring in the Upper Coal-measures. To these he gave the name of Noeggerathia spathulata and N. media. Long after, in 1879 to be exact, Dr. O. Feistmantel established his genus Noeggerathiopsis for the reception of similar leaves from the Talchir-Kararbari Beds of the Lower Gondwana System, and from his remarks it may, by inference, be concluded that Dana's were included in the new genus also. This inference is justified by Feistmantel's later definite reference of these leaves to Noeggerathiopsis; at the same time he added another species, N. prisca, from the Lower Coal-measures at Greta. He believed them to be closely allied with Cycadeaceae.


1985 ◽  
Vol 25 (1) ◽  
pp. 15
Author(s):  
P. Ties ◽  
R.D. Shaw ◽  
G.C. Geary

The Clarence-Moreton Basin covers an area of some 28 000 km2 in north-eastern New South Wales and south-eastern Queensland. The basin is relatively unexplored, with a well density in New South Wales of one per 1600 km2. Since 1980, Endeavour Resources and its co-venturers have pursued an active exploration programme which has resulted in the recognition of significant petroleum potential in the New South Wales portion of the basin.Previous studies indicated that the Upper Triassic to Lower Cretaceous Clarence-Moreton Basin sequence in general, lacked suitable reservoirs and had poor source- rock potential. While exinite rich, oil-prone source rocks were recognised in the Middle Jurassic Walloon Coal Measures, they were considered immature for oil generation. Moreover, during the 1960's the basin acquired a reputation as an area where seismic records were of poor quality.These ideas are now challenged following the results of a new round of exploration which commenced in the New South Wales portion of the basin in 1980. This exploration has involved the acquisition of over 1000 km of multifold seismic data, the reprocessing of some 200 km of existing single fold data, and the drilling of one wildcat well. Over twenty large structural leads have been identified, involving trapping mechanisms ranging from simple drape to antithetic and synthetic fault blocks associated with normal and reverse fault dependent and independent closures.The primary exploration targets in the Clarence- Moreton Basin sequence are Lower Jurassic sediments comprising a thick, porous and permeable sandstone unit in the Bundamba Group, and channel and point-bar sands in the Marburg Formation. Source rocks in these and the underlying Triassic coal measures are gas-prone and lie at maturity levels compatible with gas generation. In contrast, it was established from the results of Shannon 1 that the Walloon Coal Measures are mature for oil generation and this maturity regime is now considered to be applicable to most of the basin in New South Wales.A consideration of reservoir and source rock distribution, together with structural trends across the basin in Petroleum Exploration Licences 258 and 259, has led to the identification of three prospective fairways, two of which involve shallow oil plays. Exploration of these fairways is currently the focus of an ongoing programme of further seismic data acquisition and drilling.


Sign in / Sign up

Export Citation Format

Share Document